Observed sizes of planet-forming disks trace viscous evolution
L. Trapman, G. Rosotti, A.D. Bosman, M.R. Hogerheijde, E.F. van, Dishoeck

TL;DR
This study uses physical-chemical models to analyze how observed CO emission extents can trace viscous evolution in protoplanetary disks, revealing that current observations support viscous spreading with low disk viscosity.
Contribution
It demonstrates that CO emission extent is a valid tracer of viscous disk evolution and clarifies how physical conditions affect this observable over time.
Findings
Gas outer radius increases with disk age in viscous models
High viscosity and low disk mass can cause CO radius to decrease over time
Most observed disks in Lupus match models with low viscosity and small initial size
Abstract
The evolution of protoplanetary disks is dominated by the conservation of angular momentum, where the accretion of material onto the central star is driven by viscous expansion of the outer disk or by disk winds extracting angular momentum without changing the disk size. Studying the time evolution of disk sizes allows us therefore to distinguish between viscous stresses or disk winds as the main mechanism of disk evolution. Observationally, estimates of the disk gaseous outer radius are based on the extent of the CO rotational emission, which, during the evolution, is also affected by the changing physical and chemical conditions in the disk. We use physical-chemical DALI models to study how the extent of the CO emission changes with time in a viscously expanding disk and investigate to what degree this observable gas outer radius is a suitable tracer of viscous spreading and whether…
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